Search results for "geologia"

showing 10 items of 605 documents

Middle Triassic (Ladinian) deep-water sediments in Sicily: New findings from the Madonie Mountains

2012

A section of carbonate megabreccias grading upward to deep-water Daonella limestones is described from the locality of Sant’Otiero, near Petralia Sottana, in the Madonie Mountains (Sicily). The megabreccia mainly consists of neritic elements containing dasycladalean algae (Diplopora annulatissima Pia) along with benthic foraminifers and problematics. The overlying calcilutitic strata are characterized by lumachella intercalations containing the bivalve Daonella tyrolensis Mojsisovics suggesting an early Late Ladinian (Protrachyceras longobardicum ammonoid zone) age. We informally name the Daonella limestone as the calcare di Sant’Otiero (Sant’Otiero limestone). The Daonella limestones along…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaDaonellaStratigraphylcsh:QE1-996.5PaleontologyTriassicLadinianlcsh:Geologylcsh:PaleontologyDeep-water limestonesTriassic Ladinian Sicily Daonella deep-water limestones stratigraphy paleontologySicilylcsh:QE701-760Triassic; Ladinian; Sicily; Daonella; Deep-water limestones; Stratigraphy; Paleontology
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The Messinian salinity crisis in the Mediterranean basin: A reassessment of the data and an integrated scenario

2006

Abstract After a long period of controversial debate about the interpretation of the Messinian salinity crisis (MSC), a near consensus existed since the ODP Leg 42A for a model keeping the major lines of the deep basin-shallow water model initially proposed by Hsu et al. (1973) . The knowledge of the crisis was improved since the 1995s by the availability of a very accurate astronomically calibrated timescale. The debate about its interpretation was then reactivated by several new scenarios that questioned most the major aspects of the previous classical models. The updated re-examination of the most salient features along with consideration of the hydrological requirements for evaporite de…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaEvaporiteClimateStratigraphyScenarioGeologySettore GEO/01 - Paleontologia E Paleoecologiaengineering.materialStructural basinCauseDeposition (geology)Water levelOcean recordSedimentary depositional environmentPaleontologyMessinianErosionStage (stratigraphy)engineeringHaliteSalinity crisiGlacial periodGeologySedimentary Geology
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Fluid escape structures in the Graham Bank region (Sicily Channel, Central Mediterranean) revealing volcanic and neotectonic activity

2016

In the Sicily Channel, (Central Mediterranean), two geodynamic processes overlap each other, the Maghrebides- Apennines accretionary prism and the Sicily Channel rift. Moreover, the northwestern sector (Banks sector) is characterised by an irregular seafloor morphology linked to the recent volcanic and tectonic activity.In order to discriminate the role exerted by both the processes in the morphostructural setting of the area we used a dataset of both high and very high resolution single-channel and multi-channel profiles, acquired in the frame of the RITMARE project respectively with CHIRP and sparker, and airgun sources, and high resolution (5 m cell) morpho-bathymetric data. The data all…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaFluid escape volcanism neotectonics
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Paleoenvironmental changes heralding the Messinian Salinity Crisis in central Sicili: The Tripoli formation of the Falconara-Gibliscemi composite sec…

2004

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaForaminifera Stable isotopeMessinian Salinity CrisiSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/08 - Geochimica E Vulcanologia
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La Piattaforma Carbonatica Panormide: un caso anomalo nell'evoluzione dei bacini della Tetide giurassica

2010

Negli ultimi anni sono state proposte diverse ricostruzioni paleogeografiche dell'area Centro Mediterranea durante il Mesozoico.La Piattaforma Carbonatica Panormide (PCPA) viene collocata tra la Tetide Alpina e la Tetide Ionica, in un'area geodinamicamente molto complessa. Recenti studi hanno documentato la presenza di superfici di discontinuita che caratterizzano l'evoluzione stratigrafica della PCPA rispetto alle adiacenti Piattaforme Carbonatiche Siciliane. La presenza di superfici di discontinuita negli intervalli Retico-Hettangiano e Giurassico Medio-Oxfordiano vengono messe in relazione, attraverso il confronto della storia della subsidenza tra le Piattaforme Carbonatiche, con gli sta…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaGeneral Earth and Planetary SciencesGeologyDiscontinuità paleogeografia Piattaforma Carbonatica Panormide Sicilia subsidenza
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Guida Geologica del Parco delle Madonie - II edizione

2012

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaGeologia Parco delle Madonie SiciliaSettore GEO/04 - Geografia Fisica E GeomorfologiaSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/05 - Geologia Applicata
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Geology of the Kumeta-Pizzuta ridges (NW Sicily)

2016

We present a 1:25.000 scale geological map of the Kumeta-Pizzuta ridge in north western Sicily (Italy), which was achieved by integrating stratigraphic, structural and geophysical data. In this area the tectonic edifice results from the piling-up of deep water-, carbonate platform- and pelagic platformderived tectonic units (Imerese and Sicilide, Panormide and Trapanese domains respectively) originated by deformations of former southern Tethyan continental margin. The structural setting shows interference of subsequent tectonic events, different type of structural styles, and different-scale deformational patterns. Early overthrust of the Imerese on the Trapanese units (since late Serravall…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaGeological map Sicily Backthrust Transpressive fault
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NEOTECTONIC ACTIVITY AND EMISSION OF FLUIDS IN THE NORTHWEST SICILY CHANNEL

The southern Sicilian coast represents an important contribution to Italian tourism, the Sicily Channel is an important communication path because at the top of its seafloor there are many pipelines, and submarine communication cables which are laid to carry signals, and which are very important to the minor islands. In this work, we are presenting results of the detailed geomorphological and seismostratigraphic analysis based on new very high-resolution dataset (multibeam and CHIRP) acquired during the ACUSCAL 2015 Cruise. We also used low resolution bathymetric and seismic data provided from online database (ViDEPI, GEBCO, EMODnet). This study allows us to reconstruct the tectonic volcani…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaGraham Bank neotectonics active tectonics seamounts pockmarks mass movements mass transport deposits soft-sediment deposition structures rock falls debris avalanches volcanic and tectonics triggers Sicily Channel seepage plumes mounds active tectonics submarine volcanic edifice fluid escape.
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Geological modeling of Altavilla Milicia (Sicily) using HVSR data

2014

At today the use of inversion of HVSR curves is mainly limited to derive average parameters of the shear wave velocity, although recently they have been used also for a detailed reconstruction of the roof of the seismic bedrock (Di Stefano et al. 2014). Since ambient vibrations may contain waves travelling in all directions, as body waves and Rayleigh and Love waves, a limit of this method lies in the uncertain composition of seismic noise, in the lack of knowledge about the microseismic field and in the subjective choices regarding the data processing. This work aims to verify the potential and limits of the HVSR inversion for the purposes of geological reconstruction of the subsoil in hea…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaHVSR ellipticity shear wave velocity modelsSettore GEO/11 - Geofisica Applicata
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The Brolo Island, a lentil in the “Ocean”

2010

The north-eastern Sicily coast reflects the effects of Holocene active tectonics associated to subduction system of Ionian crust beneath the Calabrian arc (CAPUTO et alii, 1970; WESTAWAY, 1993, DOGLIONI et alii, 1999). The latter, characterized by a stack of crystalline rock and its sedimentary cover, is the highest structural element in the Sicily chain. The Calabrian arc is a region that records one of the major Quaternary vertical tectonic movement in the whole Mediterranean basin. This uplift, well documented from Last Interglacial, is expressed as vertical variation of the height of the Quaternary marine terraces inner margin that characterize the north-eastern Sicily coast. The uplift…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaHolocene Sicily sea level rise tectonics.
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